Blair H C, Kahn A J, Crouch E C, Jeffrey J J, Teitelbaum S L
J Cell Biol. 1986 Apr;102(4):1164-72. doi: 10.1083/jcb.102.4.1164.
Osteoclasts are the principal resorptive cells of bone, yet their capacity to degrade collagen, the major organic component of bone matrix, remains unexplored. Accordingly, we have studied the bone resorptive activity of highly enriched populations of isolated chicken osteoclasts, using as substrate devitalized rat bone which had been labeled in vivo with L-[5-3H]proline or 45Ca, and bone-like matrix produced and mineralized in vitro by osteoblast-like rat osteosarcoma cells. When co-cultured with a radiolabeled substrate, osteoclast-mediated mineral mobilization reached a maximal rate within 2 h, whereas organic matrix degradation appeared more slowly, reaching maximal rate by 12-24 h. Thereafter, the rates of organic and inorganic matrix resorption were essentially linear and parallel for at least 6 d when excess substrate was available. Osteoclast-mediated degradation of bone collagen was confirmed by amino acid analysis. 39% of the solubilized tritium was recovered as trans-4-hydroxyproline, 47% as proline. 10,000 osteoclasts solubilized 70% of the total radioactivity and 65% of the [3H]-trans-4-hydroxyproline from 100 micrograms of 25-50 micron bone fragments within 5 d. Virtually all released tritium-labeled protein was of low molecular weight, 99% with Mr less than or equal to 10,000, and 65% with Mr less than or equal to 1,000. Moreover, when the 14% of resorbed [3H]proline-labeled peptides with Mr greater than or equal to 2,000 were examined for the presence of TCA and TCB, the characteristic initial products of mammalian collagenase activity, none was detected by SDS PAGE. In addition, osteoclast-conditioned medium had no collagenolytic activity, and exogenous TCA and TCB fragments were not degraded by osteoclasts. On the other hand, osteoclast lysates have collagenolytic enzyme activity in acidic but not in neutral buffer, with maximum activity at pH 4.0. These data indicate that osteoclasts have the capacity to resorb the organic phase of bone by a process localized to the osteoclast and its attachment site. This process appears to be independent of secretion of neutral collagenase and probably reflects acid protease activity.
破骨细胞是骨组织主要的吸收细胞,然而它们降解骨基质主要有机成分——胶原蛋白的能力仍未得到研究。因此,我们使用在体内用L-[5-³H]脯氨酸或⁴⁵Ca标记的失活大鼠骨,以及由大鼠成骨样骨肉瘤细胞在体外产生并矿化的类骨基质作为底物,研究了高度富集的分离鸡破骨细胞群体的骨吸收活性。当与放射性标记底物共培养时,破骨细胞介导的矿物质动员在2小时内达到最大速率,而有机基质降解出现得较慢,在12 - 24小时达到最大速率。此后,当有过量底物时,有机和无机基质的吸收速率在至少6天内基本呈线性且平行。通过氨基酸分析证实了破骨细胞介导的骨胶原蛋白降解。溶解的³H中有39%以反式-4-羟脯氨酸形式回收,47%以脯氨酸形式回收。10000个破骨细胞在5天内从100微克25 - 50微米的骨碎片中溶解了70%的总放射性和65%的[³H]-反式-4-羟脯氨酸。几乎所有释放的³H标记蛋白分子量都很低,99%的Mr小于或等于10000,65%的Mr小于或等于1000。此外,当检测Mr大于或等于2000的14%的已吸收[³H]脯氨酸标记肽中是否存在哺乳动物胶原酶活性的特征性初始产物TCA和TCB时,通过SDS-PAGE未检测到任何产物。另外,破骨细胞条件培养基没有胶原olytic活性,并且外源性TCA和TCB片段也不被破骨细胞降解。另一方面,破骨细胞裂解物在酸性缓冲液中有胶原olytic酶活性,而在中性缓冲液中没有,在pH 4.0时活性最大。这些数据表明破骨细胞有能力通过一个局限于破骨细胞及其附着位点的过程吸收骨的有机相。这个过程似乎独立于中性胶原酶的分泌,可能反映了酸性蛋白酶的活性。